Soil organic carbon (SOC) constitutes a large pool within the global carbon cycle. Changes in land-use/cover strongly drive variation of SOC stocks. We analyzed the changes in four types of land use/cover and their influence on SOC content, density, and regional stocks along the main channel of the Tarim River in China for 2000-2010 obtained from remotely sensed images and field surveys. The areas and structures of the land uses/covers changed greatly during this period. Specifically, the areas of cultivated, industrial and residential, and shrub land increased, particularly cultivated and shrub land. The areas of forestland, grassland, water bodies, and unused land decreased. SOC stocks in forestland, grassland and unused land decreased be...
Land use is an important factor affecting soil organic carbon (SOC) dynamics and can produce positiv...
© 2015, Springer International Publishing Switzerland. Backgrounds and aims: Land use is an importan...
Spatial distributions of 0–20 cm soil carbon sources/sinks caused by land use changes from the year ...
Understanding the effects of land use changes on the spatiotemporal variation of soil organic carbon...
Understanding the effects of land use changes on the spatiotemporal variation of soil organic carbon...
Land use change is a key factor driving changes in soil organic carbon (SOC) around the world. Howev...
AbstractUnderstanding the effects of land use changes on the spatiotemporal variation of soil organi...
AbstractUnderstanding the effects of land use changes on the spatiotemporal variation of soil organi...
This paper uses a national-level geographic information system database on land use, weather conditi...
This paper uses a national-level geographic information system database on land use, weather conditi...
Accounting for one quarter of China’s land area, the endorheic Shiyang River basin is a vast semi-ar...
Soil organic carbon (SOC) and total nitrogen (total N) are important soil components for agricultura...
Soil carbon (C) pool contains organic carbon (SOC) and inorganic carbon (SIC). A detailed understand...
The Grain to Green Program in China which began in 1999 led to the conversion of 0.64 million ha of ...
AbstractSpatial distributions of 0–20 cm soil carbon sources/sinks caused by land use changes from t...
Land use is an important factor affecting soil organic carbon (SOC) dynamics and can produce positiv...
© 2015, Springer International Publishing Switzerland. Backgrounds and aims: Land use is an importan...
Spatial distributions of 0–20 cm soil carbon sources/sinks caused by land use changes from the year ...
Understanding the effects of land use changes on the spatiotemporal variation of soil organic carbon...
Understanding the effects of land use changes on the spatiotemporal variation of soil organic carbon...
Land use change is a key factor driving changes in soil organic carbon (SOC) around the world. Howev...
AbstractUnderstanding the effects of land use changes on the spatiotemporal variation of soil organi...
AbstractUnderstanding the effects of land use changes on the spatiotemporal variation of soil organi...
This paper uses a national-level geographic information system database on land use, weather conditi...
This paper uses a national-level geographic information system database on land use, weather conditi...
Accounting for one quarter of China’s land area, the endorheic Shiyang River basin is a vast semi-ar...
Soil organic carbon (SOC) and total nitrogen (total N) are important soil components for agricultura...
Soil carbon (C) pool contains organic carbon (SOC) and inorganic carbon (SIC). A detailed understand...
The Grain to Green Program in China which began in 1999 led to the conversion of 0.64 million ha of ...
AbstractSpatial distributions of 0–20 cm soil carbon sources/sinks caused by land use changes from t...
Land use is an important factor affecting soil organic carbon (SOC) dynamics and can produce positiv...
© 2015, Springer International Publishing Switzerland. Backgrounds and aims: Land use is an importan...
Spatial distributions of 0–20 cm soil carbon sources/sinks caused by land use changes from the year ...